Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 21
... ( Lucknow district ) are located only 15 km from each other and receive a similar amount of annual rainfall ; while Charda is located in the Terai belt with a higher annual rainfall . Intratooth variation in teeth from Charda and Lucknow ...
... ( Lucknow district ) are located only 15 km from each other and receive a similar amount of annual rainfall ; while Charda is located in the Terai belt with a higher annual rainfall . Intratooth variation in teeth from Charda and Lucknow ...
Sida 22
... Lucknow region ; although the chronological trends in 81O values ( palaeomonsoon variation ) are similar . It indicates higher rainfall in Bahraich area as compared to the Lucknow region for the past few thousand years . Moreover ...
... Lucknow region ; although the chronological trends in 81O values ( palaeomonsoon variation ) are similar . It indicates higher rainfall in Bahraich area as compared to the Lucknow region for the past few thousand years . Moreover ...
Sida 33
... Lucknow : Lucknow University . Singh , D.S. and I.B. Singh 2005. Facies Architecture of the Gandak Megafan , Ganga Plain , India , Palaeontological Society of India Special Publi- cation 2 : 125-140 . Singh , G. 1999. Review of the Work ...
... Lucknow : Lucknow University . Singh , D.S. and I.B. Singh 2005. Facies Architecture of the Gandak Megafan , Ganga Plain , India , Palaeontological Society of India Special Publi- cation 2 : 125-140 . Singh , G. 1999. Review of the Work ...
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activity Agastya agricultural alluvial ancient archaeological areas Balathal beads Bengal body calcrete cave Cedrela century Chalcolithic changes channels charcoal climate cultural dates Deccan Delhi deposits distribution district early Early Historic early medieval evidence excavations Ganga Plain geomorphic glass Harappan Historic human important increase India indicates interfluve iron known kyr BP lakes Late Later layer located Lucknow Marginal material Megafan Middle monsoon mound namely natural northern occupation origin parenchyma period phase Pleistocene ponds present produced prominent Pune Quaternary rainfall range rays record region remains ridges river sediments settlements Shankharis Sharma shells shows similar Singh slope Society soil South southern species stone structures surface Survey tanks temples thick tion tradition tree Trench University Valley vegetation vessels village wall Ware West western wood zone